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  • Tropical Atlantic  (2)
  • (8) 20/09 BELEM MARG. ESQUERDA P.1.5M 0-4; 09/05_P99; 09/05 P99 MACAPA SUL MARG. DIREITA; 101_9/5_MACAPA; 101 9/5 MACAPA SUL ESQUERDA; 12/03_MCP; 12/03 MCP NORTEE MARGEM ESQ 0-2 PONTO; 13/05/11_BELEM; 13/05/11BELEM RIO PARA P40 MEIO CANAL 04; 14/09_MCP; 14/09_MCP_MEP; 14/09 MCP MEP SUL MARG. DIREITA PTO 4 CORE 0-4; 14/09 MCP PONTO 6 0-4; 20/09_BELEM; 20/09_BELEM_MARG; 20/09_BLM; 20/09 BELEM PTO 8 MARGEM ESQ. 0-4; 20/09 BLM MD PONTO2 0-4; 25/9/11_OBIDOS; 25/9/11 OBIDOS ME CORE 0-4; 7/5_MACAPA; 7/5_P95; 7/5 MACAPA NORTE P.94 ESQUERDA; 7/5 P95 MACAPA NORTE MEIO; 9/5_MACAPA; 9/5 MACAPA SUL PIOO MEIO; Aluminium/Silicon ratio; Area/locality; Average chain length; Calculated; Carbon, organic, total; Carbon Preference Index; Center for Marine Environmental Sciences; DEPTH, sediment/rock; Element analyser CS, LECO CS-200; Elevation of event; Event label; Latitude of event; Longitude of event; Madeira River; MAO_02c; MAO_02d; MAO_02e; MAO_02f_VGRAB; MAO_03a; MAO_03h; MAO_05d_VGRAB; MAO_08a; MAO_08b; MAO_09b; MAO_11a; MAO_11c; MAO_13b; MAO_13c; MAO_23a; MAO_24a; MAO_25a; MAO_25b; MAO_25d; MAO_25e; MAO_28a; MAO_28d; MAO_3; MAO_32; MAO_4; MAO_73; MAO_77_VGRAB; MAO_90; MARUM; MCP_SUL_P89; MCP SUL P89 ESQ P-2M; MIC; MiniCorer; n-Alkane C29-C31; n-Alkane C29-C32, δ13C; n-Alkane C29-C32, δD; Negro River; Para River; Sample code/label; Season; Solimoes River; van Veen Grab; VGRAB; XA_25; XA_30; XA_31; XA_33; XA_34; XA_35; XA_36; XA_38; XA_76; Xingu River
  • Center for Marine Environmental Sciences; Leibniz Centre for Tropical Marine Research; MARUM; ZMT
  • Radiocarbon
  • 2010-2014  (3)
Document type
Keywords
Years
Year
  • 1
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2004. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Paleoceanography 19 (2004): PA4029, doi:10.1029/2003PA000892.
    Description: We compare a new mid-Pleistocene sea surface temperature (SST) record from the eastern tropical Atlantic to changes in continental ice volume, orbital insolation, Atlantic deepwater ventilation, and Southern Ocean front positions to resolve forcing mechanisms of tropical Atlantic SST during the mid-Pleistocene transition (MPT). At the onset of the MPT, a strong tropical cooling occurred. The change from a obliquity- to a eccentricity-dominated cyclicity in the tropical SST took place at about 650 kyr BP. In orbital cycles, tropical SST changes significantly preceded continental ice-volume changes but were in phase with movements of Southern Ocean fronts. After the onset of large-amplitude 100-kyr variations, additional late glacial warming in the eastern tropical Atlantic was caused by enhanced return flow of warm waters from the western Atlantic driven by strong trade winds. Pronounced 80-kyr variations in tropical SST occurred during the MPT, in phase with and likely directly forced by transitional continental ice-volume variations. During the MPT, a prominent anomalous long-term tropical warming occurred, likely generated by extremely northward displaced Southern Ocean fronts. While the overall pattern of global climate variability during the MPT was determined by changes in mean state and frequency of continental ice volume variations, tropical Atlantic SST variations were primarily driven by early changes in Subantarctic sea-ice extent and coupled Southern Ocean frontal positions.
    Description: The Dutch scientific funding organization (NWO) is thanked for financial support (project 75019617).
    Keywords: Sea surface temperatures ; Mid-Pleistocene transition ; Tropical Atlantic
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2022-05-26
    Description: Author Posting. © American Geophysical Union, 2005. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Paleoceanography 20 (2005): PA1019, doi:10.1029/2005PA001134.
    Keywords: Sea-surface temperatures ; Mid-Pleistocene transition ; Tropical Atlantic
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Location Call Number Limitation Availability
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  • 3
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    PANGAEA
    In:  Supplement to: Contreras-Rosales, Lorena Astrid; Jennerjahn, Tim C; Tharammal, Thejna; Meyer, Vera D; Lückge, Andreas; Paul, André; Schefuß, Enno (2014): Evolution of the Indian Summer Monsoon and terrestrial vegetation in the Bengal region during the past 18 ka. Quaternary Science Reviews, 102, 133-148, https://doi.org/10.1016/j.quascirev.2014.08.010
    Publication Date: 2023-03-03
    Description: The Indian Summer Monsoon (ISM) is a major global climatic phenomenon. Long-term precipitation proxy records of the ISM, however, are often fragmented and discontinuous, impeding an estimation of the magnitude of precipitation variability from the Last Glacial to the present. To improve our understanding of past ISM variability, we provide a continuous reconstructed record of precipitation and continental vegetation changes from the lower Ganges-Brahmaputra-Meghna catchment and the Indo-Burman ranges over the last 18,000 years (18 ka). The records derive from a marine sediment core from the northern Bay of Bengal (NBoB), and are complemented by numerical model results of spatial moisture transport and precipitation distribution over the Bengal region. The isotopic composition of terrestrial plant waxes (dD and d13C of n-alkanes) are compared to results from an isotope-enabled general atmospheric circulation model (IsoCAM) for selected time slices (pre-industrial, mid-Holocene and Heinrich Stadial 1). Comparison of proxy and model results indicate that past changes in the dD of precipitation and plant waxes were mainly driven by the amount effect, and strongly influenced by ISM rainfall. Maximum precipitation is detected for the Early Holocene Climatic Optimum (EHCO; 10.5-6 ka BP), whereas minimum precipitation occurred during the Heinrich Stadial 1 (HS1; 16.9-15.4 ka BP). The IsoCAM model results support the hypothesis of a constant moisture source (i.e. the NBoB) throughout the study period. Relative to the pre-industrial period the model reconstructions show 20% more rain during the mid-Holocene (6 ka BP) and 20% less rain during the Heinrich Stadial 1 (HS1), respectively. A shift from C4-plant dominated ecosystems during the glacial to subsequent C3/C4-mixed ones during the interglacial took place. Vegetation changes were predominantly driven by precipitation variability, as evidenced by the significant correlation between the dD and d13C alkane records. When compared to other records across the ISM domain, precipitation and vegetation changes inferred from our records and the numerical model results provide evidence for a coherent regional variability of the ISM from the Last Glacial to the present.
    Keywords: Center for Marine Environmental Sciences; Leibniz Centre for Tropical Marine Research; MARUM; ZMT
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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